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思茅松中幼龄人工林的生物量碳密度及其动态变化
引用本文:李江,邱琼,朱宏涛,孟梦,陈宏伟,冯弦,刘永刚,郭永清,翟明普.思茅松中幼龄人工林的生物量碳密度及其动态变化[J].中国水土保持科学,2011,9(2):106-111.
作者姓名:李江  邱琼  朱宏涛  孟梦  陈宏伟  冯弦  刘永刚  郭永清  翟明普
作者单位:1. 云南省林业科学院,650204;昆明北京林业大学,100083,北京
2. 云南省林业科学院,650204,昆明
3. 中科院昆明植物研究所,650204,昆明
4. 北京林业大学,100083,北京
基金项目:云南省应用基础研究“云南森林碳储量测算和林业碳汇潜力研究”(2007C240M); 云南省技术创新人材培养计划(2008PY085); 国家科技支撑计划“亚热带山地造林固碳技术研究”(2008BAD95B09),“小桐子人工林碳汇功能研究”(2007BAD32B02-08)
摘    要: 通过样地实测生物量和采用重铬酸钾法测定植物碳索含量,研究了思茅松中幼龄人工林生物量碳密度的分配特征及随林龄的动态变化规律。结果表明:1)林龄为3-5、6-10、11 -20和21 -30 a思茅松人工林的生物量碳密度分别为(20.15 ±3.09)、(27. 24 ±2.25)、(94. 89 ±9. 90)和147. 58 t/hm2。随林齡增长,乔木层、枯落物层和林分的碳密度显著增加,灌木层和草本层的碳密度有所减少。林分、乔木层和枯落物层的生物量碳密度随林龄的变化用逻辑斯蒂模型可实现良好拟合,而灌木层和草本层拟合效果差。2)林龄为3-5、6-10、11 -20和263思茅松人工林的年均固碳量分别为(4. 92 ±0.63)、(3. 52 ±0.25〉、(6. 44 ±0.30)和5. 68 t/(hm2·a)0乔木层的年均固碳量与林龄存在显著正相关,灌木层和草本层的年均固碳请与林龄存在显著负相关,林分年均固碳量与林龄呈较弱的正相关。乔木层和草本层的年均固碳量与林龄的关系以逻辑斯蒂模型拟合效果较好,灌木层年均固碳量和林龄关系以Gauss模型拟合效果较好,林分的年均固碳量与林龄的拟合效果差。

关 键 词:思茅松  中幼龄人工林  生物量碳密度  动态

Biomass carbon density and its dynamics for young and middle aged plantation of Pinus kesiya var. langbianensis
Li Jiang,Qiu Qiong,Zhu Hongtao,Meng Meng,Chen Hongwei,Feng Xuan,Liu Yonggang,Guo Yongqing,Zhai Mingpu.Biomass carbon density and its dynamics for young and middle aged plantation of Pinus kesiya var. langbianensis[J].Science of Soil and Water Conservation,2011,9(2):106-111.
Authors:Li Jiang  Qiu Qiong  Zhu Hongtao  Meng Meng  Chen Hongwei  Feng Xuan  Liu Yonggang  Guo Yongqing  Zhai Mingpu
Institution:Li Jiang1,2,Qiu Qiong1,Zhu Hongtao3,Meng Meng1,Chen Hongwei 1,Feng Xuan1,Liu Yonggang1,Guo Yongqing1,Zhai Mingpu2 (1.Yunnan Academy of Forestry,650204,Kunming,2.Beijing Forestry University,100083,Beijing,3.Kunming Institute of Botany,Chinese Academy of Sciences,Kunming: China)
Abstract:Based on biomass data collected from field surveys and plant carbon contents determined in laboratory,biomass carbon density and its dynamics for the young and middle aged plantation of Pinus kesiya var.langbianensis were studied.Results showed that: 1) Biomass carbon density for the plantations of age 3-5,6-10,11-20 and 26 years were(20.15±3.09),(27.24±2.25),(94.89±9.90) and 147.58t/hm2 respectively.Over stand age,biomass carbon density increased significantly for stand,arbor layer and litter layer,while decreased slightly for shrub layer and grass layer.Relations between biomass carbon density and stand age for stand,arbor layer and litter layer could be performed well by a logistic model,while the fitting effects for shrub and grass layer were not satisfied.2) Mean annual rate of biomass carbon sequestration for the plantations of age 3-5,6-10,11-20 and 26 years were(4.92±0.63),(3.52±0.25),(6.44±0.30) and 5.68t/(hm2·a) respectively.The rates were positively related to stand age for arbor layer and stand and negatively related for shrub and grass layers.The relations between the rates and stand age could be well performed by a logistic model for arbor and grass layer,and by a Gauss model for shrub layer,while the fitting effects for the relation for stand were not satisfied.
Keywords:Pinus kesiya var  langbianensis  young and middle aged plantation  biomass carbon density  dynamics  
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